1. No category

California Groundwater
Overview
Outline
•
Groundwater fundamentals
– California groundwater occurrence & general background
– Overdraft & negative consequences
•
•
•
•
•
•
•
Non-sustainable storage depletion
Subsidence
Surface water & ecosystem effects
Increased energy costs
Bad water intrusion from aquitards and from depth
Basin salt imbalance
Seawater intrusion
– Sustainable yield
•
Groundwater myths
–
–
–
–
–
–
•
Pumping of “fossil water” is non-sustainable
Groundwater storage depletion always takes a long time to recover
Groundwater levels tell us how much groundwater storage is changing
Quality of most groundwater is degraded
Good quality groundwater today is likely to stay that way
Potential myth: climate change will decrease groundwater recharge
Case studies
– Coachella Valley
– Yolo County
– Orange Co.
CA Water Use & Supply, CA Water Plan 2014
CA Water Use & Supply, CA Water Plan 2014
Groundwater Use in 1,000’s of acre-feet
~43% of Californians rely on groundwater for
drinking water
5
20,000-35,000 PWS wells
Groundwater Occurrence
8
Major Aquifers (http://nationalatlas.gov/natlas/natlasstart.asp)
Volcanics
Alluvial Valleys
Alluvial Valleys, Basin & Range
10
11
Sierra Nevada Granitics (Green Lake area, Hoover Wilderness)
aa lava flow, Newbury Crater, Oregon
Alluvial Fan (near Bozeman, Montana)
http://geology.about.com/library/bl/images/blalluvfan.htm
Kings River Fan Aquifer System
• Stream-dominated alluvial fan
system (fluvial depositional
system);
• Located southeast of Fresno,
California;
• Study area located in medial
fan area.
Kings River Alluvial Fan
San Joaquin Valley Groundwater (from Faunt, 2009)
PreDevelopment
PostDevelopment
21
Groundwater and Surface Water
From CA Water Plan 2014
Cosumnes Alluvial Aquifer System
Woodland Area Aquifer System
Network (Stephen Maples, HYD 273)
Davis Area Aquifer System Network
(Katie Markovich, HYD 273)
Groundwater
Land
surface
Unsaturated zone
Saturated zone
Water table
Surface water
Ground water
Creviced rock
Air
Water (not ground water) held by molecular attraction
Surrounds surfaces of rock particles
Gravel
Air
Approximate level of the water table
All openings below water table
full of ground water
32
Confined Aquifer Schematic (from Driscoll, 1986)
Potential energy in confined aquifer
Well
Myth: Old (1,000’s of yrs) groundwater is fossil water
that is not replenished enough to support pumping.
33
34
San Joaquin Valley Groundwater (from Faunt, 2009)
PreDevelopment
PostDevelopment
37
Groundwater Overdraft: Pumping more
groundwater than the system can sustain
Potential consequences:
• Non-sustainable storage depletion
• Subsidence
• Surface water & ecosystem effects
• Increased energy costs
• Bad water intrusion from aquitards and from
depth
• Basin salt imbalance
• Seawater intrusion
Groundwater Overdraft Trends,
Central Valley
39
From presentation JE Reager, San Gabriel Valley Water Forum held
October 2, 2014, Pomona, CA. JT Reager, CA's drought
Groundwater Overdraft: Pumping more
groundwater than the system can sustain
Potential consequences:
• Non-sustainable storage depletion
• Subsidence
• Surface water & ecosystem effects
• Increased energy costs
• Bad water intrusion from aquitards and from
depth
• Basin salt imbalance
• Seawater intrusion
Mining Ground Water
San Joaquin Valley, California
Approximate location of
maximum subsidence in the
United States identified by
Joe Poland (pictured)
43
Groundwater Overdraft: Pumping more
groundwater than the system can sustain
Potential consequences:
• Non-sustainable storage depletion
• Subsidence
• Surface water & ecosystem effects
• Increased energy costs
• Bad water intrusion from aquitards and from
depth
• Basin salt imbalance
• Seawater intrusion
47
From Alley et al. (1999)
Visualization of CA’s
Soggy Past
From
http://www.geocurren
ts.info/geonotes/visual
izing-californias-soggypast
From Faunt (2009)
49
Groundwater Overdraft: Pumping more
groundwater than the system can sustain
Potential consequences:
• Non-sustainable storage depletion
• Subsidence
• Surface water & ecosystem effects
• Increased energy costs
• Bad water intrusion from aquitards and from
depth
• Basin salt imbalance
• Seawater intrusion
Potential for Water Quality Degradation from Below is Clear and
Present, but Unaddressed
Woodland Area Aquifer System
Network (Stephen Maples, HYD 273)
Groundwater Overdraft: Pumping more
groundwater than the system can sustain
Potential consequences:
• Non-sustainable storage depletion
• Subsidence
• Surface water & ecosystem effects
• Increased energy costs
• Bad water intrusion from aquitards and from
depth
• Basin salt imbalance
• Seawater intrusion
The danger of a
hydrologic
basin losing its
outlet….
San Joaquin Valley Groundwater (from Faunt, 2009)
PreDevelopment
PostDevelopment
56
Groundwater Overdraft: Pumping more
groundwater than the system can sustain
Potential consequences:
• Non-sustainable storage depletion
• Subsidence
• Surface water & ecosystem effects
• Increased energy costs
• Bad water intrusion from aquitards and from
depth
• Basin salt imbalance
• Seawater intrusion
58
Groundwater
Quality is
Degrading in Many
Systems,
But Most of the
Groundwater
Quality is Still Good
Age Distribution & Sustainability:
Groundwater Ages are Highly Mixed!
This means that if we see contamination
in the groundwater today, and if that
contamination is from a persistent, nonpoint source, we can expect decades to
centuries of worsening groundwater
quality.
63
Groundwater quality sustainability is one of
the major scientific and societal issues of our
time...
•
•
64
Most fresh groundwater resources are 102 - 103 yr old, yet most
anthropogenic contaminants <50-60 yr old.
– Especially in western alluvial basins, Gulf Coast, Atlantic coastal
plain, etc.
– Not so much in shallow, glacio-fluvial outwash, moist climates?
Groundwater ages (even from short screens) are generally highly mixed.
– Molecular ages typically range greatly (e.g., 101 - 102 or 103 yr)
within a single sample (Fogg et al., 1999; Tompson et al., 1999;
Weissmann et al., 2002; Bethke & Johnson, 2002).
– In other words, in many systems there is significant potential for
water quality to get much worse over the coming decades to
centuries, depending on contaminant sources.
64
65
USDA National Water Meeting
May 23, 2012
Presented by Doug Parker, Univ of California
Thomas Harter & Jay Lund, Principal Investigators
Jeannie Darby, Graham Fogg, Richard Howitt, Katrina
Jessoe, Jim Quinn, Stu Pettygrove, Joshua Viers,
Co-Investigators
http://groundwaternitrate.ucdavis.edu
Aaron King, Allan Hollander, Alison McNally, Anna
Fryjoff-Hung, Cathryn Lawrence, Daniel Liptzin, Danielle
Dolan, Dylan Boyle, Elena Lopez, Giorgos Kourakos,
Holly Canada, Josue Medellin-Azuara, Kristin Dzurella,
Kristin Honeycutt, Megan Mayzelle, Mimi Jenkins, Nicole
de la Mora, Todd Rosenstock, Vivian Jensen,
Researchers
Watershed Science Center
University of California, Davis
Contact: ThHarter@ucdavis.edu
Historic Nitrate Trends, TLB:
Exceedance Rate
Percent of wells above natural background
Number of wells tested
Percent of wells above half nitrate MCL
Percent of wells above nitrate MCL
Year
A Look at Davis, CA
City of Davis, CA Well Data, <135 m Depth
Major confining layers present
Davis
UCD and City of Davis Well
Screened Intervals
UCD drinking water
wells
UCD utility water wells
City deep water wells
City of Davis Groundwater Levels, Intermediate-Depth Aquifer
Online plots from Elizabeth Case
City of Davis Groundwater Levels, Deep Aquifer
Online plots from Elizabeth Case
Trend in UCD Drinking Water Wells (Deep Aquifer)
Trend in UCD Utility (landscape and ?) Wells
(Intermediate-depth Aquifer)
Case Study: Coachella Valley
Groundwater Systems:
Work with Harvey O. Banks
during 1987-96
Graham E. Fogg
76
77
78
79
80
81
82
83
Overview of Orange County Water
District’s Managed Aquifer Recharge
System
Recharge System Tour
Slides Courtesy of Roy Herndon and Adam Hutchinson,
OCWD
Overview of Orange County Water
District’s Managed Aquifer Recharge
System
Recharge System Tour
Slides Courtesy of Roy Herndon and Adam
Hutchinson, OCWD
The Orange County groundwater basin lies at
the base of the Santa Ana River watershed.
• Longest coastal riverThe
in Southern
California
Santa
Ana River Watershed
• 130 km from highest mountains
to Pacific Ocean
Mojave Desert
San
• Watershed
covers 690,000 hectares
Gabriel
Mtns..
San Bernardino Mtns.
Chino
Basin
San
Bernardino
Basin
Los
Angeles
Orange
County
Basin
Santa Ana
River
P acific
Ocean
Santa
Ana
Mtns.
San
Jacinto
Mtns.
Over the course of 75 years, the District has
purchased 600 hectares for recharge.
1936-1947
1958
1963-68
1970-79
1983-85
2003-04
2010
Basin geology limits the area where
surface MAR can be used.
North
South
Recharge Area
Pressure Area
0m
SHALLOW AQUIFER
300 m
PRINCIPAL AQUIFER
600 m
DEEP AQUIFER
NON-WATERBEARING
FORMATION
900 m
0 km
8
16
24
Most groundwater production is from the Principal Aquifer.
32
Orange Co., CA (Tompson, Carle,
Rosenberg, and Maxwell, 1999)
The Anaheim Lake complex covers 60 hectares
and can recharge SAR, imported and recycled
water.
Miraloma Basin
(4 ha)
Kraemer Basin
(12 ha)
Miller Basin
(10 ha)
Recycled Water
Anaheim Lake
(28 ha)
SAR Water
Imported Water
Over the past decade, surface water recharge has
averaged 274 million m3 per year from a variety of
sources.
350
300
250
Annual
200
Recharge
(million m3/yr) 150
100
GWRS
Imported/Purchased Water
Storm Flow
Base Flow
50
1936
1940
1944
1948
1952
1956
1960
1964
1968
1972
1976
1980
1984
1988
1992 *
1996 *
2000 *
2004*
2008*
2012*
0
Year
(1936-1990 is Oct-Sept water year, 1991-2012 is July-June Fiscal Year)
Outline
•
Groundwater fundamentals
– California groundwater occurrence & general background
– Overdraft & negative consequences
•
•
•
•
•
•
•
Non-sustainable storage depletion
Subsidence
Surface water & ecosystem effects
Increased energy costs
Bad water intrusion from aquitards and from depth
Basin salt imbalance
Seawater intrusion
– Sustainable yield
•
Groundwater myths
–
–
–
–
–
–
•
Pumping of “fossil water” is non-sustainable
Groundwater storage depletion always takes a long time to recover
Groundwater levels tell us how much groundwater storage is changing
Quality of most groundwater is degraded
Good quality groundwater today is likely to stay that way
Potential myth: climate change will decrease groundwater recharge
Case studies
– Coachella Valley
– Yolo County
– Orange Co.
Confined Aquifer Schematic (from Driscoll, 1986)
Potential energy in confined aquifer
Well
Myth: Old (1,000’s of yrs) groundwater is fossil water
that is not replenished enough to support pumping.
94
Groundwater and Surface Water
From CA Water Plan 2014